3D fault imaging using windowed Radon transforms: an example from the North Sea
3D fault imaging using windowed Radon transforms: an example from the North Sea
The interpretation of fault surfaces is key to understanding the subsurface geology represented in 3D seismic volumes. The geologic structure represented by seismic reflections can be auto-tracked in the volume. Faults, however, are imaged as discontinuities or changes in curvature in the seismic data ...